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The name Natalus stramineus has been historically applied to populations of the genus Natalus from virtually the entire Neotropics. The geographic origin of the holotype of N. stramineus, however, has never been known with certainty, confounding discussions concerning the species limits, nomenclature, and biogeography of this genus. The type locality of N. stramineus was assumed to be Brazil for about 80 years, but was later transferred to the Lesser Antilles. Although the later view has dominated the taxonomy of Natalus for the past four decades, there have been recent claims that the type locality might indeed be in Brazil. In this study, I provide morphological evidence that corroborates the Lesser Antillean origin of the holotype of N. stramineus. In addition, I argue that N. stramineus-like populations do not occur in northern South America implying that the genus Natalus is distributed throughout Central and South America as three allopatric taxa. The findings presented here prompt the recognition of two additional species for the continental Neotropics and put and end to lingering confusion about the degree of sympatry, or lack thereof, among these species. Finally, I summarize the available information about the natural history of N. stramineus, as herein restricted, and argue that the current distribution of the species is likely the result of ancestral dispersal from northern South America.
Here we report a right dentary of Peter's ghost-faced bat Mormoops megalophylla from an archeological site in northern Matanzas province, western Cuba. The specimen was excavated from a pre-Columbian archeological cave deposit in association with stone tools, bivalve shells, snake and fish vertebrae, and capromyid (rodent) postcranial elements. Although the deposit is not directly dated, the relationship of the assemblage to the time of Amerindian occupation in this cave suggests an age between 1600 and 850 years BP Therefore, this report may constitute a probable ‘last occurrence’ date for M. megalophylla in Cuba. This bat is believed to have gone extirpated in the West Indies because of a combination of habitat-area loss due to climatic turnover during the late Pleistocene and human disturbance later in the Holocene. Based on new evidence, we add that climate-related bat extirpations could lag for several thousands of years after the onset of new environmental conditions, and that these can be easily accelerated by anthropogenic disturbance. This information can help improve the understanding of chiropteran diversity, causes, and timing of extirpations in Cuba and the West Indies.
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